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DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

DICTIONARY OF GEOPHYSICS, ASTROPHYSICS, and ASTRONOMY

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orbit around the sun, are stable points in a three<br />

body system (sun – planet – asteriod). For the<br />

case of the planet Jupiter, a number of asteriods<br />

have been found in this region <strong>and</strong> are all named<br />

after heroes of the Trojan wars.<br />

Trojans asteroids Asteroids located near<br />

Jupiter’s Lagrange points (60 ◦ ahead <strong>and</strong> behind<br />

Jupiter in its orbit).<br />

tropical cyclone A large low pressure system<br />

that originates over the tropical oceans; including<br />

tropical depressions, tropical storms,<br />

<strong>and</strong> hurricanes (cyclones, typhoons), with winds<br />

sometimes up to 300 km/h.<br />

tropical instability waves Oceanic disturbances<br />

of meridional scale of 500 km, zonal<br />

wavelength of 1000 km <strong>and</strong> a period of 30 days<br />

that travel westward along 2-3 ◦ N in the equatorial<br />

Atlantic <strong>and</strong> Pacific Oceans. Instabilities of<br />

velocity shears among equatorial currents are<br />

their cause. They start to grow in June <strong>and</strong><br />

decay toward the end of a year, in correlation<br />

with the intensity of equatorial currents. They<br />

are well visible from satellite infrared images<br />

as they cause me<strong>and</strong>ers of a strong sea surface<br />

temperature (SST) front between the equator<br />

<strong>and</strong> 5 ◦ N. Often called the Legeckis waves after<br />

the discoverer of the waves’ signature in SST.<br />

These wave-induced SST variations excite atmospheric<br />

waves of significant amplitudes in the<br />

marine boundary layer.<br />

tropical month See month.<br />

tropical storm A storm originating in the<br />

tropics; particularly severe tropical storms become<br />

hurricanes (sustained wind speeds ><br />

120 km/h).<br />

tropical year See year.<br />

Tropic of Cancer The parallel of latitude<br />

23 ◦ 27 ′ N. The sun lies in the zenith (overhead<br />

at noon) at this latitude, at the summer solstice,<br />

around June 22. North of this latitude, the sun<br />

is always south of directly overhead.<br />

Tropic of Capricorn The parallel of latitude<br />

23 ◦ 27 ′ S. The sun lies in the zenith (overhead<br />

© 2001 by CRC Press LLC<br />

trough<br />

at noon) at this latitude, at the winter solstice,<br />

around December 22. South of this latitude, the<br />

sun is always north of directly overhead.<br />

tropopause The boundary layer between the<br />

troposphere <strong>and</strong> the stratosphere. In the troposphere,<br />

air temperature generally decreases<br />

with height, <strong>and</strong> in the lower parts of the stratosphere,<br />

air temperature remains constant or increases<br />

(0.1 to 0.2 ◦ C/100 m). The altitude of<br />

the tropopause varies with the variations of sea<br />

— surface temperature, season, latitude, <strong>and</strong><br />

weather systems, such as the passage of cyclones<br />

<strong>and</strong> anti-cyclones. It has its highest<br />

height (about 17 to 18 km) over the equator<br />

<strong>and</strong> lowest (about 6 to 8 km, average 10 to<br />

12 km) over the poles. There are two different<br />

types of tropopause. One is the pole-region<br />

tropopause with height lower than 150 hPa; another<br />

is the tropical-subtropical tropopause with<br />

height higher than 150 hPa. Because of this<br />

distinct height difference, when these two different<br />

types of air mass systems approach, the<br />

tropopause will appear as a broken phenomenon.<br />

Under such a broken tropopause, there is<br />

often a high level jet which is related to the front.<br />

troposphere The layer of the atmosphere<br />

closest to the planet’s surface. The troposphere<br />

is characterized by a decrease in temperature<br />

with altitude, caused by a decrease in the amount<br />

of warming due to the Greenhouse Effect with<br />

altitude. Hadley Cell circulation <strong>and</strong> the Greenhouse<br />

Effect dominate the temperature profile<br />

<strong>and</strong> weather patterns within the troposphere. On<br />

Earth, the troposphere extends to about 25 km<br />

above the surface. The exact height varies with<br />

latitude <strong>and</strong> season. The boundary between the<br />

troposphere <strong>and</strong> the stratosphere is called the<br />

tropopause. The troposphere is also often called<br />

the lower atmosphere.<br />

trough A long, relatively wide trough running<br />

on sea bottoms, whose maximum depth of<br />

the water is less than 6000 m. This definition<br />

is applied irrespective of the origin of troughs.<br />

There are some troughs whose structure <strong>and</strong> origin<br />

are basically the same as those of trenches.<br />

Such an example is the Nankai trough situated<br />

on the Pacific side of the Japanese isl<strong>and</strong>s. For<br />

such a trough, as is the case for a trench, seismic<br />

487

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